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Peak metamorphic conditions during the Alpine chloritoid-forming event reached 3. The chemistry of the chloritoid schists bears the signature of upper continental crustal felsic rocks as potential protoliths, probably the felsic rocks of the nearby Papuk Complex of Slavonian Mts.
The evidence presented here for the chloritoid-bearing low-grade metamorphic rocks from the Slavonian Mountains clearly show that the prograde Alpine metamorphic event had a more significant influence on the evolution of the southern part of Tisia Mega-Unit than previously considered.
Part of Springer Nature. Not logged in Not affiliated Phase equilibrium, geothermobarometric and xenotime age dating constraints on the Alpine metamorphism recorded in chloritoid schists from the southern part of the Tisia Mega-Unit Slavonian Mts. Original Paper First Online: Anders E, Grevesse N Abundances of the elements: Geochim Cosmochim Acta Rev Mineral Geochem Acta Geol Hung Int J Earth Sci PhD thesis, University of Zagreb, pp in Croatian Google Scholar.
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Cite this article as: Int J Earth Sci Geol Rundsch RIS Papers Reference Manager RefWorks Zotero. BIB BibTeX JabRef Mendeley.
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